{"version":"1.0","provider_name":"International Institute of Earthquake Engineering and Seismology","provider_url":"https:\/\/www.iiees.ac.ir\/en","title":"The Zagros mountain range: Structural evolution and seismicity - International Institute of Earthquake Engineering and Seismology","type":"rich","width":600,"height":338,"html":"<blockquote class=\"wp-embedded-content\" data-secret=\"OXiMSpCNBW\"><a href=\"https:\/\/www.iiees.ac.ir\/en\/the-zagros-mountain-range-structural-evolution-and-seismicity\/\">The Zagros mountain range: Structural evolution and seismicity<\/a><\/blockquote><iframe sandbox=\"allow-scripts\" security=\"restricted\" src=\"https:\/\/www.iiees.ac.ir\/en\/the-zagros-mountain-range-structural-evolution-and-seismicity\/embed\/#?secret=OXiMSpCNBW\" width=\"600\" height=\"338\" title=\"&#8220;The Zagros mountain range: Structural evolution and seismicity&#8221; &#8212; International Institute of Earthquake Engineering and Seismology\" data-secret=\"OXiMSpCNBW\" frameborder=\"0\" marginwidth=\"0\" marginheight=\"0\" scrolling=\"no\" class=\"wp-embedded-content\"><\/iframe><script>\n\/*! This file is auto-generated *\/\n!function(d,l){\"use strict\";l.querySelector&&d.addEventListener&&\"undefined\"!=typeof URL&&(d.wp=d.wp||{},d.wp.receiveEmbedMessage||(d.wp.receiveEmbedMessage=function(e){var t=e.data;if((t||t.secret||t.message||t.value)&&!\/[^a-zA-Z0-9]\/.test(t.secret)){for(var s,r,n,a=l.querySelectorAll('iframe[data-secret=\"'+t.secret+'\"]'),o=l.querySelectorAll('blockquote[data-secret=\"'+t.secret+'\"]'),c=new RegExp(\"^https?:$\",\"i\"),i=0;i<o.length;i++)o[i].style.display=\"none\";for(i=0;i<a.length;i++)s=a[i],e.source===s.contentWindow&&(s.removeAttribute(\"style\"),\"height\"===t.message?(1e3<(r=parseInt(t.value,10))?r=1e3:~~r<200&&(r=200),s.height=r):\"link\"===t.message&&(r=new URL(s.getAttribute(\"src\")),n=new URL(t.value),c.test(n.protocol))&&n.host===r.host&&l.activeElement===s&&(d.top.location.href=t.value))}},d.addEventListener(\"message\",d.wp.receiveEmbedMessage,!1),l.addEventListener(\"DOMContentLoaded\",function(){for(var e,t,s=l.querySelectorAll(\"iframe.wp-embedded-content\"),r=0;r<s.length;r++)(t=(e=s[r]).getAttribute(\"data-secret\"))||(t=Math.random().toString(36).substring(2,12),e.src+=\"#?secret=\"+t,e.setAttribute(\"data-secret\",t)),e.contentWindow.postMessage({message:\"ready\",secret:t},\"*\")},!1)))}(window,document);\n\/\/# sourceURL=https:\/\/www.iiees.ac.ir\/en\/wp-includes\/js\/wp-embed.min.js\n<\/script>\n","description":"The Zagros fold-thrust belt, which extends for approximately 1600 kilometers from the Taurus mountains in northeastern Turkey, the Kurdistan region in northern Iraq, and southwestern Iran, continues to the Strait of Hormoz, with a northwest-southeast orientation. The northeastern boundary of the Zagros belt is marked by the Main Zagros fault, which separates the Senjed-Sirjan zone [&hellip;]","thumbnail_url":"https:\/\/www.iiees.ac.ir\/en\/wp-content\/uploads\/2024\/10\/1.png","thumbnail_width":1347,"thumbnail_height":1235}